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    ΠœΠ˜Π“Π ΠΠ¦Π˜Π― Π‘Π•Π™Π‘ΠœΠ˜Π§Π•Π‘ΠšΠžΠ™ И Π’Π£Π›ΠšΠΠΠ˜Π§Π•Π‘ΠšΠžΠ™ ΠΠšΠ’Π˜Π’ΠΠžΠ‘Π’Π˜ КАК ΠŸΠ ΠžΠ―Π’Π›Π•ΠΠ˜Π• Π’ΠžΠ›ΠΠžΠ’ΠžΠ“Πž Π“Π•ΠžΠ”Π˜ΠΠΠœΠ˜Π§Π•Π‘ΠšΠžΠ“Πž ΠŸΠ ΠžΠ¦Π•Π‘Π‘Π

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    Publications about the earthquake foci migration have been reviewed. An importantΒ result of such studies is establishment of wave nature of seismic activity migration that isΒ manifested by two types of rotational waves; such waves are responsible for interactionΒ between earthquakes foci and propagate with different velocities. Waves determiningΒ long-range interaction of earthquake foci are classified as Type 1; their limiting velocitiesΒ range from 1 to 10 cm/s. Waves determining short-range interaction of foreshocks andΒ aftershocks of individual earthquakes are classified as Type 2; their velocities range fromΒ 1 to 10 km/s. According to the classification described in [Bykov, 2005], these two typesΒ of migration waves correspond to slow and fast tectonic waves.Β The most complete data on earthquakes (for a period over 4.1 million of years) andΒ volcanic eruptions (for 12 thousand years) of the planet are consolidated in a unifiedΒ systematic format and analyzed by methods developed by the authors. For the PacificΒ margin, Alpine-Himalayan belt and the Mid-Atlantic Ridge, which are the three mostΒ active zones of the Earth, new patterns of spatial and temporal distribution of seismic andΒ volcanic activity are revealed; they correspond to Type 1 of rotational waves. The waveΒ nature of the migration of seismic and volcanic activity is confirmed. A new approach toΒ solving problems of geodynamics is proposed with application of the data on migrationΒ of seismic and volcanic activity, which are consolidated in this study, in combination withΒ data on velocities of movement of tectonic plate boundaries. This approach is based onΒ the concept of integration of seismic, volcanic and tectonic processes that develop in theΒ block geomedium and interact with each other through rotating waves with a symmetricΒ stress tensor. The data obtained in this study give grounds to suggest that a geodynamicΒ value, that is mechanically analogous to an impulse, remains constant in such interactions.Β It is thus shown that the process of wave migration of geodynamic activity should beΒ described by models with strongly nonlinear equations of motion.ΠŸΡ€ΠΎΠ²Π΅Π΄Π΅Π½ ΠΎΠ±Π·ΠΎΡ€ Ρ€Π°Π±ΠΎΡ‚ ΠΏΠΎ ΠΌΠΈΠ³Ρ€Π°Ρ†ΠΈΠΈ ΠΎΡ‡Π°Π³ΠΎΠ² зСмлСтрясСний. Π’Π°ΠΆΠ½Ρ‹ΠΌ Ρ€Π΅Π·ΡƒΠ»ΡŒΡ‚Π°Ρ‚ΠΎΠΌΒ ΡΠ²ΠΈΠ»ΠΎΡΡŒ установлСниС Π²ΠΎΠ»Π½ΠΎΠ²ΠΎΠΉ ΠΏΡ€ΠΈΡ€ΠΎΠ΄Ρ‹ ΠΌΠΈΠ³Ρ€Π°Ρ†ΠΈΠΈ сСйсмичСской активности, которая осущСствляСтся  двумя Ρ‚ΠΈΠΏΠ°ΠΌΠΈ Ρ€ΠΎΡ‚Π°Ρ†ΠΈΠΎΠ½Π½Ρ‹Ρ… Π²ΠΎΠ»Π½, отвСтствСнными за взаимодСйствиС ΠΎΡ‡Π°Π³ΠΎΠ² зСмлСтрясСний ΠΈ Ρ€Π°ΡΠΏΡ€ΠΎΡΡ‚Ρ€Π°Π½ΡΡŽΡ‰ΠΈΠΌΠΈΡΡ с Ρ€Π°Π·Π½Ρ‹ΠΌΠΈ скоростями. ΠŸΠ΅Ρ€Π²ΠΎΠΌΡƒ Ρ‚ΠΈΠΏΡƒ с ΠΏΡ€Π΅Π΄Π΅Π»ΡŒΠ½Ρ‹ΠΌΠΈ скоростями 1–10 см/с ΡΠΎΠΎΡ‚Π²Π΅Ρ‚ΡΡ‚Π²ΡƒΡŽΡ‚ Π²ΠΎΠ»Π½Ρ‹,Β ΠΎΠΏΡ€Π΅Π΄Π΅Π»ΡΡŽΡ‰ΠΈΠ΅ Π΄Π°Π»ΡŒΠ½ΠΎΠ΄Π΅ΠΉΡΡ‚Π²ΡƒΡŽΡ‰Π΅Π΅ взаимодСйствиС ΠΎΡ‡Π°Π³ΠΎΠ² зСмлСтрясСний, Π²Ρ‚ΠΎΡ€ΠΎΠΌΡƒ – с ΠΏΡ€Π΅Π΄Π΅Π»ΡŒΠ½Ρ‹ΠΌΠΈ скоростями 1–10 ΠΊΠΌ/с – ΡΠΎΠΎΡ‚Π²Π΅Ρ‚ΡΡ‚Π²ΡƒΡŽΡ‚ Π²ΠΎΠ»Π½Ρ‹, ΠΎΠΏΡ€Π΅Π΄Π΅Π»ΡΡŽΡ‰ΠΈΠ΅Β Π±Π»ΠΈΠ·ΠΊΠΎΠ΄Π΅ΠΉΡΡ‚Π²ΡƒΡŽΡ‰Π΅Π΅ взаимодСйствиС Ρ„ΠΎΡ€ΡˆΠΎΠΊΠΎΠ² ΠΈ Π°Ρ„Ρ‚Π΅Ρ€ΡˆΠΎΠΊΠΎΠ² Π² ΠΏΡ€Π΅Π΄Π΅Π»Π°Ρ… ΠΎΡ‚Π΄Π΅Π»ΡŒΠ½ΠΎΒ Π²Π·ΡΡ‚Ρ‹Ρ… ΠΎΡ‡Π°Π³ΠΎΠ² зСмлСтрясСний. Богласно классификации [Bykov, 2005], Ρ‚Π°ΠΊΠΈΠ΅ Ρ‚ΠΈΠΏΡ‹Β Π²ΠΎΠ»Π½ ΠΌΠΈΠ³Ρ€Π°Ρ†ΠΈΠΈ ΡΠΎΠΎΡ‚Π²Π΅Ρ‚ΡΡ‚Π²ΡƒΡŽΡ‚ ΠΌΠ΅Π΄Π»Π΅Π½Π½Ρ‹ΠΌ ΠΈ быстрым тСктоничСским Π²ΠΎΠ»Π½Π°ΠΌ.Β Π’ Π΅Π΄ΠΈΠ½ΠΎΠΌ Ρ„ΠΎΡ€ΠΌΠ°Ρ‚Π΅ прСдставлСны Π½Π°ΠΈΠ±ΠΎΠ»Π΅Π΅ ΠΏΠΎΠ»Π½Ρ‹Π΅ Π΄Π°Π½Π½Ρ‹Π΅ ΠΎ зСмлСтрясСниях Π·Π°Β 4.1 тыс. Π»Π΅Ρ‚ ΠΈ извСрТСниях Π²ΡƒΠ»ΠΊΠ°Π½ΠΎΠ² Π·Π° 12 тыс. Π»Π΅Ρ‚. Π‘ΠΎΠ±Ρ€Π°Π½Π½Ρ‹Π΅ Π΄Π°Π½Π½Ρ‹Π΅ систСматизированы ΠΈ ΠΏΡ€ΠΎΠ°Π½Π°Π»ΠΈΠ·ΠΈΡ€ΠΎΠ²Π°Π½Ρ‹ с ΠΏΠΎΠΌΠΎΡ‰ΡŒΡŽ Ρ€Π°Π·Ρ€Π°Π±ΠΎΡ‚Π°Π½Π½Ρ‹Ρ… Π°Π²Ρ‚ΠΎΡ€Π°ΠΌΠΈ ΠΌΠ΅Ρ‚ΠΎΠ΄ΠΈΠΊ. Для Ρ‚Ρ€Π΅Ρ… Π½Π°ΠΈΠ±ΠΎΠ»Π΅Π΅ Π°ΠΊΡ‚ΠΈΠ²Π½Ρ‹Ρ… поясов Π—Π΅ΠΌΠ»ΠΈ – ΠŸΠ°Ρ†ΠΈΡ„ΠΈΠΊΠΈ, Альпийско-Гималайского и Π‘Ρ€Π΅Π΄ΠΈΠ½Π½ΠΎ-АтлантичСского – установлСны Π½ΠΎΠ²Ρ‹Π΅, ΠΎΡ‚Π²Π΅Ρ‡Π°ΡŽΡ‰ΠΈΠ΅ ΠΏΠ΅Ρ€Π²ΠΎΠΌΡƒ Ρ‚ΠΈΠΏΡƒ Ρ€ΠΎΡ‚Π°Ρ†ΠΈΠΎΠ½Π½Ρ‹Ρ… Π²ΠΎΠ»Π½, закономСрности пространствСнно-Π²Ρ€Π΅ΠΌΠ΅Π½Π½ΠΎΠ³ΠΎ распрСдСлСния сСйсмичСской ΠΈ вулканичСской активности. ΠŸΠΎΠ΄Ρ‚Π²Π΅Ρ€ΠΆΠ΄Π΅Π½Π° волновая ΠΏΡ€ΠΈΡ€ΠΎΠ΄Π° ΠΈΡ…Β ΠΌΠΈΠ³Ρ€Π°Ρ†ΠΈΠΈ. ΠŸΠΎΠ»ΡƒΡ‡Π΅Π½Π½Ρ‹Π΅ Π² Ρ€Π°Π±ΠΎΡ‚Π΅ Π΄Π°Π½Π½Ρ‹Π΅ Π² совокупности с Π΄Π°Π½Π½Ρ‹ΠΌΠΈ ΠΎ скоростях двиТСния Π³Ρ€Π°Π½ΠΈΡ† тСктоничСских ΠΏΠ»ΠΈΡ‚ прСдлагаСтся ΠΈΡΠΏΠΎΠ»ΡŒΠ·ΠΎΠ²Π°Ρ‚ΡŒ Π² качСствС Π½ΠΎΠ²ΠΎΠ³ΠΎ ΠΏΠΎΠ΄Ρ…ΠΎΠ΄Π° ΠΊ Ρ€Π΅ΡˆΠ΅Π½ΠΈΡŽ Π·Π°Π΄Π°Ρ‡ Π³Π΅ΠΎΠ΄ΠΈΠ½Π°ΠΌΠΈΠΊΠΈ. Π’ основС Ρ‚Π°ΠΊΠΎΠ³ΠΎ ΠΏΠΎΠ΄Ρ…ΠΎΠ΄Π° залоТСна идСя Сдинства сСйсмичСского, вулканичСского ΠΈ тСктоничСского процСссов, ΠΏΡ€ΠΎΡ‚Π΅ΠΊΠ°ΡŽΡ‰ΠΈΡ… Π² Π±Π»ΠΎΠΊΠΎΠ²ΠΎΠΉ гСосрСдС ΠΈ Π²Π·Π°ΠΈΠΌΠΎΠ΄Π΅ΠΉΡΡ‚Π²ΡƒΡŽΡ‰ΠΈΡ… ΠΌΠ΅ΠΆΠ΄Ρƒ собой посрСдством ротационных Π²ΠΎΠ»Π½ с симмСтричным Ρ‚Π΅Π½Π·ΠΎΡ€ΠΎΠΌ напряТСний. ΠŸΠΎΠ»ΡƒΡ‡Π΅Π½Π½Ρ‹Π΅ Π°Π²Ρ‚ΠΎΡ€Π°ΠΌΠΈ Π΄Π°Π½Π½Ρ‹Π΅ ΠΏΠΎΠ·Π²ΠΎΠ»ΡΡŽΡ‚ ΠΏΡ€Π΅Π΄ΠΏΠΎΠ»ΠΎΠΆΠΈΡ‚ΡŒ, Ρ‡Ρ‚ΠΎ ΠΏΡ€ΠΈ Ρ‚Π°ΠΊΠΎΠΌ взаимодСйствии сохраняСтся гСодинамичСская Π²Π΅Π»ΠΈΡ‡ΠΈΠ½Π°, мСханичСским Π°Π½Π°Π»ΠΎΠ³ΠΎΠΌ ΠΊΠΎΡ‚ΠΎΡ€ΠΎΠΉ являСтся ΠΈΠΌΠΏΡƒΠ»ΡŒΡ. Показано, Ρ‡Ρ‚ΠΎ процСсс Π²ΠΎΠ»Π½ΠΎΠ²ΠΎΠΉ ΠΌΠΈΠ³Ρ€Π°Ρ†ΠΈΠΈ гСодинамичСской активности Π΄ΠΎΠ»ΠΆΠ΅Π½Β ΠΎΠΏΠΈΡΡ‹Π²Π°Ρ‚ΡŒΡΡ Π² Ρ€Π°ΠΌΠΊΠ°Ρ… ΠΌΠΎΠ΄Π΅Π»Π΅ΠΉ с сильно Π½Π΅Π»ΠΈΠ½Π΅ΠΉΠ½Ρ‹ΠΌΠΈ уравнСниями двиТСния

    НСсСзонноС производство ягодной ΠΏΡ€ΠΎΠ΄ΡƒΠΊΡ†ΠΈΠΈ ΠΌΠ°Π»ΠΈΠ½Ρ‹ красной Π² условиях ΠΎΡ‚Π°ΠΏΠ»ΠΈΠ²Π°Π΅ΠΌΡ‹Ρ… Π·ΠΈΠΌΠ½ΠΈΡ… Ρ‚Π΅ΠΏΠ»ΠΈΡ†

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    Relevance. Currently, in many countries of the world, the production of non-season raspberry berry products has become widespread. Recently, interest in this technology has arisen in Russia, which has great prospects for the development of industrial gardening. In our opinion, it is promising to develop elements of technology for the non-seasonal production of red raspberries, propagated by the method of clonal micropropagation with a traditional and remontant type of fruiting in the conditions of winter heated greenhouses.Material and methods. The experiments were carried out in the laboratory of clonal micropropagation of garden plants in the fruit growing laboratory of RGAU-MSHA named after K.A. Timiryazev. The objects of research were varieties of red raspberries with a traditional (variety Volnitsa) and remontant (varieties Orangevoe Chudo and Bryanskoe Divo) type of fruiting. The experimental plants were propagated by the method of clonal micropropagation and grown before distillation in open and protected ground; plants propagated by root offspring served as control. Experimental plants were planted in open ground for growing in mid-May, in mid-October they were transplanted into 10 liter containers and transferred to protected ground conditions. Then put in the refrigerator compartment with a temperature of + 1 ... + 5Β°C. For distillation, the raspberry repairing plants were exposed in the winter heated greenhouse on January 20, while the shoots of replacing the aboveground system were normalized: without normalization, 3 shoots per plant, complete pruning of the aboveground system. Raspberries with a traditional type of fruiting were exposed in a winter heated greenhouse in three periods on January 20, February 10, March 2. Accounting for the passage of the phenological phases of development and yield was made for 3 months every 5 days.Results. In the conditions of winter heated greenhouses, efficiency has been shown and elements of technology for non-season production of raspberry berries remontant and berries with a traditional type of fruiting, propagated in vitro and grown before open field distillation are developed. It was revealed that it is necessary to normalize the shoots before distillation of raspberry remontant, and the optimal timing for the start of distillation for raspberries with a traditional type of fruiting has been established.ΠΠΊΡ‚ΡƒΠ°Π»ΡŒΠ½ΠΎΡΡ‚ΡŒ. Π’ настоящСС врСмя Π²ΠΎ ΠΌΠ½ΠΎΠ³ΠΈΡ… странах ΠΌΠΈΡ€Π° ΡˆΠΈΡ€ΠΎΠΊΠΎΠ΅ распространСниС ΠΏΠΎΠ»ΡƒΡ‡ΠΈΠ»ΠΎ производство нСсСзонной ягодной ΠΏΡ€ΠΎΠ΄ΡƒΠΊΡ†ΠΈΠΈ ΠΌΠ°Π»ΠΈΠ½Ρ‹. Π’ послСднСС врСмя интСрСс ΠΊ Π΄Π°Π½Π½ΠΎΠΉ Ρ‚Π΅Ρ…Π½ΠΎΠ»ΠΎΠ³ΠΈΠΈ Π²ΠΎΠ·Π½ΠΈΠΊ ΠΈ Π² России, Ρ‡Ρ‚ΠΎ ΠΈΠΌΠ΅Π΅Ρ‚ большиС пСрспСктивы для развития ΠΏΡ€ΠΎΠΌΡ‹ΡˆΠ»Π΅Π½Π½ΠΎΠ³ΠΎ садоводства. На наш взгляд, пСрспСктивно Ρ€Π°Π·Ρ€Π°Π±Π°Ρ‚Ρ‹Π²Π°Ρ‚ΡŒ элСмСнты Ρ‚Π΅Ρ…Π½ΠΎΠ»ΠΎΠ³ΠΈΠΈ нСсСзонного производства ягод ΠΌΠ°Π»ΠΈΠ½Ρ‹ красной, Ρ€Π°Π·ΠΌΠ½ΠΎΠΆΠ΅Π½Π½ΠΎΠΉ ΠΌΠ΅Ρ‚ΠΎΠ΄ΠΎΠΌ клонального микроразмноТСния с Ρ‚Ρ€Π°Π΄ΠΈΡ†ΠΈΠΎΠ½Π½Ρ‹ΠΌ ΠΈ Ρ€Π΅ΠΌΠΎΠ½Ρ‚Π°Π½Ρ‚Π½Ρ‹ΠΌ Ρ‚ΠΈΠΏΠΎΠΌ плодоношСния Π² условиях Π·ΠΈΠΌΠ½ΠΈΡ… ΠΎΡ‚Π°ΠΏΠ»ΠΈΠ²Π°Π΅ΠΌΡ‹Ρ… Ρ‚Π΅ΠΏΠ»ΠΈΡ†.ΠœΠ°Ρ‚Π΅Ρ€ΠΈΠ°Π» ΠΈ ΠΌΠ΅Ρ‚ΠΎΠ΄ΠΈΠΊΠ°. ΠžΠΏΡ‹Ρ‚Ρ‹ ΠΏΡ€ΠΎΠ²ΠΎΠ΄ΠΈΠ»ΠΈ Π² Π»Π°Π±ΠΎΡ€Π°Ρ‚ΠΎΡ€ΠΈΠΈ клонального микроразмноТСния садовых растСний Π»Π°Π±ΠΎΡ€Π°Ρ‚ΠΎΡ€ΠΈΠΈ плодоводства РГАУ-МБΠ₯А ΠΈΠΌ. К.А. ВимирязСва. ΠžΠ±ΡŠΠ΅ΠΊΡ‚Π°ΠΌΠΈ исслСдований слуТили сорта ΠΌΠ°Π»ΠΈΠ½Ρ‹ красной с Ρ‚Ρ€Π°Π΄ΠΈΡ†ΠΈΠΎΠ½Π½Ρ‹ΠΌ (сорт Π’ΠΎΠ»ΡŒΠ½ΠΈΡ†Π°) ΠΈ Ρ€Π΅ΠΌΠΎΠ½Ρ‚Π°Π½Ρ‚Π½Ρ‹ΠΌ (сорта ΠžΡ€Π°Π½ΠΆΠ΅Π²ΠΎΠ΅ Ρ‡ΡƒΠ΄ΠΎ ΠΈ БрянскоС Π΄ΠΈΠ²ΠΎ) Ρ‚ΠΈΠΏΠΎΠΌ плодоношСния. ΠžΠΏΡ‹Ρ‚Π½Ρ‹Π΅ растСния Π±Ρ‹Π»ΠΈ Ρ€Π°Π·ΠΌΠ½ΠΎΠΆΠ΅Π½Ρ‹ ΠΌΠ΅Ρ‚ΠΎΠ΄ΠΎΠΌ клонального микроразмноТСния ΠΈ Π²Ρ‹Ρ€Π°Ρ‰Π΅Π½Ρ‹ ΠΏΠ΅Ρ€Π΅Π΄ Π²Ρ‹Π³ΠΎΠ½ΠΊΠΎΠΉ Π² ΠΎΡ‚ΠΊΡ€Ρ‹Ρ‚ΠΎΠΌ ΠΈ Π·Π°Ρ‰ΠΈΡ‰Π΅Π½Π½ΠΎΠΌ Π³Ρ€ΡƒΠ½Ρ‚Π΅, ΠΊΠΎΠ½Ρ‚Ρ€ΠΎΠ»Π΅ΠΌ слуТили растСния, Ρ€Π°Π·ΠΌΠ½ΠΎΠΆΠ΅Π½Π½Ρ‹Π΅ ΠΊΠΎΡ€Π½Π΅Π²Ρ‹ΠΌΠΈ отпрысками. Π’ ΠΎΡ‚ΠΊΡ€Ρ‹Ρ‚Ρ‹ΠΉ Π³Ρ€ΡƒΠ½Ρ‚ растСния Π±Ρ‹Π»ΠΈ высаТСны Π² сСрСдинС мая, Π² сСрСдинС октября ΠΈΡ… пСрСсадили Π² ΠΊΠΎΠ½Ρ‚Π΅ΠΉΠ½Π΅Ρ€Ρ‹ объСмом 10 Π» ΠΈ пСрСнСсли Π² условия Π·Π°Ρ‰ΠΈΡ‰Π΅Π½Π½ΠΎΠ³ΠΎ Π³Ρ€ΡƒΠ½Ρ‚Π°. Π—Π°Ρ‚Π΅ΠΌ выставили Π² Ρ…ΠΎΠ»ΠΎΠ΄ΠΈΠ»ΡŒΠ½Ρ‹ΠΉ отсСк с Ρ‚Π΅ΠΌΠΏΠ΅Ρ€Π°Ρ‚ΡƒΡ€ΠΎΠΉ 1…5Β°C. Для Π²Ρ‹Π³ΠΎΠ½ΠΊΠΈ растСния ΠΌΠ°Π»ΠΈΠ½Ρ‹ Ρ€Π΅ΠΌΠΎΠ½Ρ‚Π°Π½Ρ‚Π½ΠΎΠΉ выставляли Π² зимнюю ΠΎΡ‚Π°ΠΏΠ»ΠΈΠ²Π°Π΅ΠΌΡƒΡŽ Ρ‚Π΅ΠΏΠ»ΠΈΡ†Ρƒ 20 января, ΠΏΡ€ΠΈ этом ΠΏΡ€ΠΎΠΈΠ·Π²ΠΎΠ΄ΠΈΠ»ΠΈ Π½ΠΎΡ€ΠΌΠΈΡ€ΠΎΠ²ΠΊΡƒ ΠΏΠΎΠ±Π΅Π³ΠΎΠ² замСщСния Π½Π°Π΄Π·Π΅ΠΌΠ½ΠΎΠΉ систСмы: Π±Π΅Π· Π½ΠΎΡ€ΠΌΠΈΡ€ΠΎΠ²ΠΊΠΈ, 3 ΠΏΠΎΠ±Π΅Π³Π° Π½Π° растСниС, полная ΠΎΠ±Ρ€Π΅Π·ΠΊΠ° Π½Π°Π΄Π·Π΅ΠΌΠ½ΠΎΠΉ систСмы. ΠœΠ°Π»ΠΈΠ½Ρƒ с Ρ‚Ρ€Π°Π΄ΠΈΡ†ΠΈΠΎΠ½Π½Ρ‹ΠΌ Ρ‚ΠΈΠΏΠΎΠΌ плодоношСния выставляли Π² зимнюю ΠΎΡ‚Π°ΠΏΠ»ΠΈΠ²Π°Π΅ΠΌΡƒΡŽ Ρ‚Π΅ΠΏΠ»ΠΈΡ†Ρƒ Π² Ρ‚Ρ€ΠΈ срока 20 января, 10 фСвраля, 2 ΠΌΠ°Ρ€Ρ‚Π°. Π£Ρ‡Π΅Ρ‚Ρ‹ прохоТдСния фСнологичСских Ρ„Π°Π· развития ΠΈ поступлСния уроТая ΠΏΡ€ΠΎΠΈΠ·Π²ΠΎΠ΄ΠΈΠ»ΠΈ Π² Ρ‚Π΅Ρ‡Π΅Π½ΠΈΠ΅ 3 мСсяцСв Ρ‡Π΅Ρ€Π΅Π· ΠΊΠ°ΠΆΠ΄Ρ‹Π΅ 5 Π΄Π½Π΅ΠΉ.Π Π΅Π·ΡƒΠ»ΡŒΡ‚Π°Ρ‚Ρ‹. Π’ условиях Π·ΠΈΠΌΠ½ΠΈΡ… ΠΎΡ‚Π°ΠΏΠ»ΠΈΠ²Π°Π΅ΠΌΡ‹Ρ… Ρ‚Π΅ΠΏΠ»ΠΈΡ† ΠΏΠΎΠΊΠ°Π·Π°Π½Π° ΡΡ„Ρ„Π΅ΠΊΡ‚ΠΈΠ²Π½ΠΎΡΡ‚ΡŒ ΠΈ Ρ€Π°Π·Ρ€Π°Π±ΠΎΡ‚Π°Π½Ρ‹ элСмСнты Ρ‚Π΅Ρ…Π½ΠΎΠ»ΠΎΠ³ΠΈΠΈ нСсСзонного производства ягод ΠΌΠ°Π»ΠΈΠ½Ρ‹ Ρ€Π΅ΠΌΠΎΠ½Ρ‚Π°Π½Ρ‚Π½ΠΎΠΉ ΠΈ с Ρ‚Ρ€Π°Π΄ΠΈΡ†ΠΈΠΎΠ½Π½Ρ‹ΠΌ Ρ‚ΠΈΠΏΠΎΠΌ плодоношСния, Ρ€Π°Π·ΠΌΠ½ΠΎΠΆΠ΅Π½Π½Ρ‹Ρ… in vitro ΠΈ Π²Ρ‹Ρ€Π°Ρ‰Π΅Π½Π½Ρ‹Ρ… ΠΏΠ΅Ρ€Π΅Π΄ Π²Ρ‹Π³ΠΎΠ½ΠΊΠΎΠΉ Π² ΠΎΡ‚ΠΊΡ€Ρ‹Ρ‚ΠΎΠΌ Π³Ρ€ΡƒΠ½Ρ‚Π΅. ВыявлСно, Ρ‡Ρ‚ΠΎ Π½Π΅ΠΎΠ±Ρ…ΠΎΠ΄ΠΈΠΌΠΎ провСсти Π½ΠΎΡ€ΠΌΠΈΡ€ΠΎΠ²ΠΊΡƒ ΠΏΠΎΠ±Π΅Π³ΠΎΠ² ΠΏΠ΅Ρ€Π΅Π΄ Π²Ρ‹Π³ΠΎΠ½ΠΊΠΎΠΉ ΠΌΠ°Π»ΠΈΠ½Ρ‹ Ρ€Π΅ΠΌΠΎΠ½Ρ‚Π°Π½Ρ‚Π½ΠΎΠΉ ΠΈ установлСны ΠΎΠΏΡ‚ΠΈΠΌΠ°Π»ΡŒΠ½Ρ‹Π΅ сроки Π½Π°Ρ‡Π°Π»Π° Π²Ρ‹Π³ΠΎΠ½ΠΊΠΈ для ΠΌΠ°Π»ΠΈΠ½Ρ‹ с Ρ‚Ρ€Π°Π΄ΠΈΡ†ΠΈΠΎΠ½Π½Ρ‹ΠΌ Ρ‚ΠΈΠΏΠΎΠΌ плодоношСния

    MIGRATION OF SEISMIC AND VOLCANIC ACTIVITY AS DISPLAY OF WAVE GEODYNAMIC PROCESS

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    Publications about the earthquake foci migration have been reviewed. An importantΒ result of such studies is establishment of wave nature of seismic activity migration that isΒ manifested by two types of rotational waves; such waves are responsible for interactionΒ between earthquakes foci and propagate with different velocities. Waves determiningΒ long-range interaction of earthquake foci are classified as Type 1; their limiting velocitiesΒ range from 1 to 10 cm/s. Waves determining short-range interaction of foreshocks andΒ aftershocks of individual earthquakes are classified as Type 2; their velocities range fromΒ 1 to 10 km/s. According to the classification described in [Bykov, 2005], these two typesΒ of migration waves correspond to slow and fast tectonic waves.Β The most complete data on earthquakes (for a period over 4.1 million of years) andΒ volcanic eruptions (for 12 thousand years) of the planet are consolidated in a unifiedΒ systematic format and analyzed by methods developed by the authors. For the PacificΒ margin, Alpine-Himalayan belt and the Mid-Atlantic Ridge, which are the three mostΒ active zones of the Earth, new patterns of spatial and temporal distribution of seismic andΒ volcanic activity are revealed; they correspond to Type 1 of rotational waves. The waveΒ nature of the migration of seismic and volcanic activity is confirmed. A new approach toΒ solving problems of geodynamics is proposed with application of the data on migrationΒ of seismic and volcanic activity, which are consolidated in this study, in combination withΒ data on velocities of movement of tectonic plate boundaries. This approach is based onΒ the concept of integration of seismic, volcanic and tectonic processes that develop in theΒ block geomedium and interact with each other through rotating waves with a symmetricΒ stress tensor. The data obtained in this study give grounds to suggest that a geodynamicΒ value, that is mechanically analogous to an impulse, remains constant in such interactions.Β It is thus shown that the process of wave migration of geodynamic activity should beΒ described by models with strongly nonlinear equations of motion

    Non-season production of raspberry of red berry products in conditions of heated winter greenhouses

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    Relevance. Currently, in many countries of the world, the production of non-season raspberry berry products has become widespread. Recently, interest in this technology has arisen in Russia, which has great prospects for the development of industrial gardening. In our opinion, it is promising to develop elements of technology for the non-seasonal production of red raspberries, propagated by the method of clonal micropropagation with a traditional and remontant type of fruiting in the conditions of winter heated greenhouses.Material and methods. The experiments were carried out in the laboratory of clonal micropropagation of garden plants in the fruit growing laboratory of RGAU-MSHA named after K.A. Timiryazev. The objects of research were varieties of red raspberries with a traditional (variety Volnitsa) and remontant (varieties Orangevoe Chudo and Bryanskoe Divo) type of fruiting. The experimental plants were propagated by the method of clonal micropropagation and grown before distillation in open and protected ground; plants propagated by root offspring served as control. Experimental plants were planted in open ground for growing in mid-May, in mid-October they were transplanted into 10 liter containers and transferred to protected ground conditions. Then put in the refrigerator compartment with a temperature of + 1 ... + 5Β°C. For distillation, the raspberry repairing plants were exposed in the winter heated greenhouse on January 20, while the shoots of replacing the aboveground system were normalized: without normalization, 3 shoots per plant, complete pruning of the aboveground system. Raspberries with a traditional type of fruiting were exposed in a winter heated greenhouse in three periods on January 20, February 10, March 2. Accounting for the passage of the phenological phases of development and yield was made for 3 months every 5 days.Results. In the conditions of winter heated greenhouses, efficiency has been shown and elements of technology for non-season production of raspberry berries remontant and berries with a traditional type of fruiting, propagated in vitro and grown before open field distillation are developed. It was revealed that it is necessary to normalize the shoots before distillation of raspberry remontant, and the optimal timing for the start of distillation for raspberries with a traditional type of fruiting has been established
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